Hydrological and thermodynamic controls on late Holocene gypsum formation by mixing saline groundwater and Dead Sea brine

• Large gypsum capes and gypsum mounds are exposed along the retreating shores of the Dead Sea. • Gypsum was formed by “outsalting” – mixing of sulfate-bearing brines with variable salinities. • The gypsum structures were formed during periods of regional aridity and low lake level.

Gespeichert in:
Autor*in:

Weber, Nurit [verfasserIn]

Antler, Gilad

Lazar, Boaz

Stein, Mordechai

Yechieli, Yoseph

Gavrieli, Ittai

Format:

E-Artikel

Sprache:

Englisch

Erschienen:

2022

Schlagwörter:

Lacustrine Gypsum

Brines

Thermodynamic modeling

Saline springs

Outsalting

Dead Sea

Hydroclimate

Umfang:

21

Übergeordnetes Werk:

Enthalten in: 109 Discovery of Novel DNA Methylation Markers for the Detection of Colorectal Neoplasia: Selection by Methylome-Wide Analysis - Taylor, William R. ELSEVIER, 2014, journal of the Geochemical Society and the Meteoritical Society, New York, NY [u.a.]

Übergeordnetes Werk:

volume:316 ; year:2022 ; day:1 ; month:01 ; pages:363-383 ; extent:21

Links:

Volltext

DOI / URN:

10.1016/j.gca.2021.10.002

Katalog-ID:

ELV055911544

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